{"title":"朱利叶斯-哈斯特和高山湖泊起源的发现。","authors":"George Hook","doi":"10.1080/00033790.2024.2304332","DOIUrl":null,"url":null,"abstract":"<p><p>This article investigates Haast's claim that in March 1862 he independently reached the same controversial conclusion as Ramsay, that lake basins in previously glaciated regions were formed by ancient glaciers. Both men's views fuelled a passionate debate in British scientific societies. However, science historians largely ignore Haast's contribution or imply he knew about Ramsay's 'theory' before coming to a conclusion about Southern Alps lakes.To assess whether Haast independently reached that conclusion in March 1862, field records, correspondence, reports, newspaper articles, and scientific publications are examined. Of significance are communications with geologists Hochstetter, Hector, and Ramsay, botanist Hooker, and physicist Tyndall. Consideration of what Haast observed in March 1862 is also critical.However, Haast's 1862 conclusion differs from Ramsay's. While Ramsay was convinced ancient glaciers scooped out rock basins, resulting in deep lakes, Haast believed ancient retreating glaciers left moraines that dammed valleys, resulting in shallow lakes. Regardless of their differences, after Haast read Ramsay's paper in 1864, he applied Ramsay's 'theory' to New Zealand's alpine lakes and proposed an excavation process.The essence of both Ramsay's and Haast's conclusions has been confirmed by research in formerly glaciated regions worldwide. However, Haast's contribution to glaciology is overlooked or underemphasized, and warrants being more widely acknowledged.</p>","PeriodicalId":8086,"journal":{"name":"Annals of Science","volume":" ","pages":"133-173"},"PeriodicalIF":0.9000,"publicationDate":"2025-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Julius Haast and the discovery of the origin of alpine lakes.\",\"authors\":\"George Hook\",\"doi\":\"10.1080/00033790.2024.2304332\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p><p>This article investigates Haast's claim that in March 1862 he independently reached the same controversial conclusion as Ramsay, that lake basins in previously glaciated regions were formed by ancient glaciers. Both men's views fuelled a passionate debate in British scientific societies. However, science historians largely ignore Haast's contribution or imply he knew about Ramsay's 'theory' before coming to a conclusion about Southern Alps lakes.To assess whether Haast independently reached that conclusion in March 1862, field records, correspondence, reports, newspaper articles, and scientific publications are examined. Of significance are communications with geologists Hochstetter, Hector, and Ramsay, botanist Hooker, and physicist Tyndall. Consideration of what Haast observed in March 1862 is also critical.However, Haast's 1862 conclusion differs from Ramsay's. While Ramsay was convinced ancient glaciers scooped out rock basins, resulting in deep lakes, Haast believed ancient retreating glaciers left moraines that dammed valleys, resulting in shallow lakes. Regardless of their differences, after Haast read Ramsay's paper in 1864, he applied Ramsay's 'theory' to New Zealand's alpine lakes and proposed an excavation process.The essence of both Ramsay's and Haast's conclusions has been confirmed by research in formerly glaciated regions worldwide. However, Haast's contribution to glaciology is overlooked or underemphasized, and warrants being more widely acknowledged.</p>\",\"PeriodicalId\":8086,\"journal\":{\"name\":\"Annals of Science\",\"volume\":\" \",\"pages\":\"133-173\"},\"PeriodicalIF\":0.9000,\"publicationDate\":\"2025-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Annals of Science\",\"FirstCategoryId\":\"98\",\"ListUrlMain\":\"https://doi.org/10.1080/00033790.2024.2304332\",\"RegionNum\":3,\"RegionCategory\":\"哲学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"2024/2/5 0:00:00\",\"PubModel\":\"Epub\",\"JCR\":\"Q2\",\"JCRName\":\"HISTORY & PHILOSOPHY OF SCIENCE\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Annals of Science","FirstCategoryId":"98","ListUrlMain":"https://doi.org/10.1080/00033790.2024.2304332","RegionNum":3,"RegionCategory":"哲学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2024/2/5 0:00:00","PubModel":"Epub","JCR":"Q2","JCRName":"HISTORY & PHILOSOPHY OF SCIENCE","Score":null,"Total":0}
Julius Haast and the discovery of the origin of alpine lakes.
This article investigates Haast's claim that in March 1862 he independently reached the same controversial conclusion as Ramsay, that lake basins in previously glaciated regions were formed by ancient glaciers. Both men's views fuelled a passionate debate in British scientific societies. However, science historians largely ignore Haast's contribution or imply he knew about Ramsay's 'theory' before coming to a conclusion about Southern Alps lakes.To assess whether Haast independently reached that conclusion in March 1862, field records, correspondence, reports, newspaper articles, and scientific publications are examined. Of significance are communications with geologists Hochstetter, Hector, and Ramsay, botanist Hooker, and physicist Tyndall. Consideration of what Haast observed in March 1862 is also critical.However, Haast's 1862 conclusion differs from Ramsay's. While Ramsay was convinced ancient glaciers scooped out rock basins, resulting in deep lakes, Haast believed ancient retreating glaciers left moraines that dammed valleys, resulting in shallow lakes. Regardless of their differences, after Haast read Ramsay's paper in 1864, he applied Ramsay's 'theory' to New Zealand's alpine lakes and proposed an excavation process.The essence of both Ramsay's and Haast's conclusions has been confirmed by research in formerly glaciated regions worldwide. However, Haast's contribution to glaciology is overlooked or underemphasized, and warrants being more widely acknowledged.
期刊介绍:
Annals of Science , launched in 1936, publishes work on the history of science, technology and medicine, covering developments from classical antiquity to the late 20th century. The Journal has a global reach, both in terms of the work that it publishes, and also in terms of its readership. The editors particularly welcome submissions from authors in Asia, Africa and South America.
Each issue contains research articles, and a comprehensive book reviews section, including essay reviews on a group of books on a broader level. Articles are published in both English and French, and the Journal welcomes proposals for special issues on relevant topics.
The Editors and Publisher are committed to supporting early career researchers, and award an annual prize to the best submission from current doctoral students, or those awarded a doctorate in the past four years.